Gravity indicator of rheological properties of the tectonosphere of the Russian Far East

Formal indicators of the existence of spatially isolated layers characterized by the absence of sources of intense gravity anomalies in them are revealed in the tectonosphere of the eastern Baikal region, the Amur region, the Sea of Okhotsk, Kamchatka, and northeastern Russia. A stable correlation of these layers with thermal, high electrical conductivity, and lower seismic velocity anomalies implies that they are related to rheologically weakened zones of the tectonosphere, i.e., layers of lower viscosity or higher plasticity or fluidity. Minimum vertical gradients of the surface density of spherical sources of gravity anomalies, equivalent to density inhomogeneities of the compaction class, are gravitational indicators of these zones.